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| 1 | Toxofilin upregulates the host cortical actin cytoskeleton dynamics facilitating Toxoplasma invasion显示文摘 | V.Delorme-Walker M.Abrivard V.Lagal K.Anderson A.Perazzi V.Gonzalez C.Page J.Chauvet W.Ochoa N.Volkmann D.Hanein I.Tardieux | | 0，，18： | 1 |
| 2 | Concentration–discharge patterns of weathering products from global rivers显示文摘Quantifying the functional relationships relating river discharge and weathering products places key constraints on the negative feedback between the silicate weathering and climate. In this study we analyze the concentration–discharge relationships of weathering products from global rivers using previously compiled time-series datasets for concentrations and discharge from global rivers. To analyze the nature of the covariation between specific discharge and concentrations, we use both a power law equation and a recently developed solute production equation. The solute production equation allows us to quantify weathering efficiency, or the resistance to dilution at high runoff, via the Damko¨hler coefficient. These results are also compared to those derived using average concentration–discharge pairs.Both the power law exponent and the Damk?hler coefficient increase and asymptote as catchments exhibit increasingly chemostatic behavior, resulting in an inverse relationship between the two parameters. We also show that using thedistribution of average concentration–discharge pairs from global rivers, rather than fitting concentration–discharge relationships for each individual river, underestimates global median weathering efficiency by up to a factor of ~10. This study demonstrates the utility of long time-series sampling of global rivers to elucidate controlling processes needed to quantify patterns in global silicate weathering rates. | Daniel E.Ibarra Seulgi Moon Jeremy K.Caves C.Page Chamberlain Kate Maher | 2017 | Acta Geochimica2017，36，3： | 0 |
| 3 | 由变质石榴石均匀化作用推断地壳冷却速率显示文摘本文提出了一个封闭体系扩散模型,来描述由于化学相互扩散球状晶体发生均匀化作用。结合相互扩散系数的知识,就可能模拟特定岩石的温度-时间(T-t)史。作者用该模型描述了新罕布什尔西南部多期变质地体中富铁铝的石榴石均匀化作用。分析结果表明,所计算的冷却速率受区域变形史控制,特别受等温面褶皱作用控制。所提出的模型普遍适用于变质岩和固相线下火成岩的冷却问题。 | Gregory E.Muncill C.Page Chamberlain 吴志勤 | 1989 | 地质科学译丛1989，，1： | 0 |
| 4 | 变形对变质作用压力-温度径迹的影响显示文摘以褶皱和逆冲断层为主构造区的压力-温度(P-T)径迹可能是复杂的,在一个变质带内可能变化很大.P—T径迹的复杂变化,是由于褶皱作用和逆冲作用造成的热水平对流、变形期间及变形后发生的热传导,以及褶皱和逆冲断层内相对短时间的热驰豫所造成的.在褶皱区,可以观察到背斜与邻近向斜具有不同的P-T径迹,背斜内是冷却径迹,而向科内是加热径迹,这些不同P—T径迹是由于变形期间发生等温线的褶皱作用,变形后又发生等温线验豫所造成的.在多期变形褶皱区,非共轴褶皱作用造成变形带短距离(<15km)内复杂的P-T径迹,这是因为在每个褶皱作用事件中,重复发生等温线的褶皱作用以及驰豫过程.在逆冲断层为主的构造区,大型逆冲席体的P一T径迹之间存在差异,因为在变形期间从较热的逆掩席体向较冷的下盘发生热传递.逆冲作用期间的热传递引起上盘冷却,下盘加热.在发育多重逆冲席体的地区,P-T径迹可能是复杂的,它将取决于逆冲席体间的热传递速率与逆冲断层发育的相对同步性.本文讨论的褶皱和逆冲断层地区所观察到的P一T径迹,记录了10~5~10~6年的相对短时间间隔.由于小尺度的热扰动会引起矿物平衡,在一个变质带的短距离内,P-T径迹可能变化很大.因此,将P-T径迹用于恢复构造历史之前,必须进行构造及岩石学的双重研究. | C.Page Chamberlain 李江海 | 1990 | 地质科技情报1990，9，2： | 0 |
| 5 | Potassium channel blockers restore axonal conduction in CNS trauma and diseases显示文摘Myelin damage in the central nervous system(CNS)plays an important role in motor and sensory dysfunction(Shi and Sun,2011).This neuropathology is observed widely in neurotrauma such as spinal cord injuries(SCI)and is also a distinguishing feature of many neurological diseases such as multiple sclerosis(MS)and amyotrophic lateral sclerosis(ALS)(Shi and Sun,2011).Damage to myelin structure leads to severe | Jessica C.Page Riyi Shi | 2016 | Neural Regeneration Research2016，11，8： | 0 |
| 6 | 区域变质作用研究的新思路——对新英格兰阿巴拉契亚山的研究显示文摘在最近的10年中,查明造山运动期间的热过程,是地球物理学家、岩石学家和地质年代学家的基本目标。如果区域变质作用反映了岩石圈的热状态和性质的深部变化,那么,通过研究区域变质岩就有可能建立造山运动的热性状。沿着这条线索,地质年代学家与岩石学家密切合作,经研究表明,在变质作用过程中,变质作用的温度、压力随时间而变化。同时,地球物理学家利用理论热模式计算造山带热历史,结果表明,埋藏史、抬升和侵蚀、地幔热流以及地壳热形成之间具有一定的关系。以上两种方法目前都已引入到造山带变质作用和构造历史的研究之中。 | C.Page Chamberlain Haward W.Day 刘厚祥 | 1990 | 地质科学译丛1990，7，2： | 0 |
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